Equatorial electrojet current density turbulent reduction

Authors

  • Matías de la Vega Dept, de Fis., Fac. de Ciencias Exactas y Naturales, Universidad de Buenos Aires

Keywords:

direct interaction approximation, equatorial electrojet

Abstract

It was shown in a previous paper that turbulence reduces the equatorial electrojet current density at noontime. This problem is further analyzed by computing the turbulence level in the long wavelength region of the spectrum using Kraichnan's direct interaction approximation (DIA). The self-consistent equations for the electrojet current density and turbulence level are solved; the current density thus obtained fits in well with experimental data.

Downloads

Download data is not yet available.

References

Bowes, K. L., B.B. Balsey, and R. Cohen, J. Geophys. Res., 63, 2485, 1963.

Davis, T. N., K. Burrows, and J. D. Stolaris, J. Geophys. Res., 72, 1845, 1967.

de la Vega, M., and S. Duhau, J. Geophys. Res., 94, 12505, 1989.

Fejer, B. J. and M. C. Kelley, Rev. Geophys. 18, 401, 1980.

Kudeki, E., B. G. Fejer, D. T. Farley, and C. Hanuise, J. Gephs. Res., 92, 13561, 1987.

Kudeki, E., D. T. Farley, and B. G. Fejer, J. Geophys. Res., 90, 429, 1985.

Richmond, A. D., J. Atmos. Terr. Phys., 35, 1083, 1973.

Rogister, A., J. Geophys. Res., 76, 775, 1971.

Schmidt, M. J., and S. P. Gary, J. Gephys. Res., 78, 8261, 1973.

Sudan, R. N., J. Geophys. Res., 88, 4853, 1983.

Downloads

Published

1993-12-12

How to Cite

de la Vega, M. (1993). Equatorial electrojet current density turbulent reduction. Geoacta, 20, 11–17. Retrieved from https://revistas.unlp.edu.ar/geoacta/article/view/13697

Issue

Section

Scientific work